Queensland, the second largest of Australia’s states, occupies nearly one-fourth of the continent. The state is more than twice the size of the U.S. state of Texas and seven times larger than the United Kingdom. In terms of land occupancy, however, Queensland is indeed Australia’s largest state, with an occupied area greater than that of the whole of Western Australia. It also is the most decentralized mainland state, with most of its people scattered along the eastern coastline over a distance of 1,400 miles (2,250 km). The rest of the population is dispersed thinly over almost all of the vast interior, posing severe access and communication challenges. With its large area and small population, Queensland’s economy is essentially resource-based, its exports predominantly pastoral, agricultural, and mineral products.

More than half of Queensland lies north of the Tropic of Capricorn, and the early Europeans there, unfamiliar with life in the tropics, experienced much adversity in their initial attempts to colonize the region. However, the climate, formerly a handicap, eventually became an advantage. In contemporary times Queensland—under the self-proclaimed title of the “Sunshine State”—has reaped the benefits of rapid growth in tourism, some attractions being sandy surfing beaches, verdant estuaries, picturesque islands, and the Great Barrier Reef, extending for 1,250 miles (2,000 km) off Queensland’s Coral Sea coastline. The state also experienced rapid population growth through “sunbelt” migration to the more attractive coastal regions, although the population in the already sparsely populated interior continued to decline. Area 668,207 square miles (1,730,648 square km). Population (2011) 4,332,739.

Land

Relief and drainage

Queensland lies astride two major Australian landform zones: the Eastern Uplands and the Central Sedimentary Lowlands.

The eastern third of the state is a complex zone of old, eroded highlands, with extensive exposures of granite and mineralized metamorphic rocks, occasionally capped by younger basalt flows, and with broad basins of even more-recent sedimentary rocks. The boldest topography lies close to the seaboard, with summits from 2,000 to 5,000 feet (600 to 1,500 metres). The uplands attract high rainfall, supplying short, steep perennial streams, and are flanked by narrow coastal valleys. Elsewhere east of the mountains are vast sedimentary basins, forming lowlands drained by such major intermittent streams as the Burdekin, Fitzroy, Barron, and Burnett rivers. The coastline presents a variety of landscapes, including bold headlands, sandy beaches, lagoons, estuaries, wetlands, alluvial plains, occasional extensive vegetated dunelands, and a scattering of nearshore islands of great recreational value.

In contrast to the variety of the coastal area is the seeming monotony of the vast inland plains, broken occasionally by low tablelands and ranges and drained by unreliable streams that are prone to extensive flooding. Gentle gradients contribute to wide, braided stream channels, most fully developed in the Channel Country of the far southwest. These plains are underlain by the recent, deep sediments of the Great Artesian Basin, which constitutes a reliable source of water for livestock. To the northwest of the basin are the stumps of ancient mineralized uplands, forming the Mount Isa block.

Soils

Most soils are old and infertile, deficient in phosphorus and nitrogen. A lack of organic matter, particularly in arid and semiarid areas, accentuates the problem, and many soils have low capacity to absorb and retain moisture. In coastal areas the most fertile soils are of relatively recent alluvial or volcanic origin, while the gray-brown and black cracking clays of the central inland lowlands support extensive grasslands.

Climate

Lying between the low latitudes of 10° and 29° S, Queensland experiences tropical and subtropical climatic conditions. Summer temperatures are high, with average January maxima from 82 °F (28 °C) on the coast to 99 °F (37 °C) in the interior. Winters are mild and sunny, with July maxima from 68 °F (20 °C) in the south to 79 °F (26 °C) in the north. The interior experiences the most prolonged summer heat, while the southern interior and highlands have cooler winters, with a frost period of up to 100 days.

Precipitation and humidity show a persistent decline from the coast to the interior. A narrow coastal zone receives 30 to 60 inches (750 to 1,525 mm) annually, declining to only 5 to 6 inches (125 to 150 mm) in the southwest. Particularly in the northern tropics, the rainfall is concentrated in a wet season extending through summer and early autumn. Southern Queensland receives sufficient winter rain to support winter cropping of wheat. A limited coastal zone in northern Queensland receives copious year-round rainfall from the prevailing southeast winds, with annual totals of up to 180 inches (4,575 mm). Rainfall is highly variable, with extremes of drought and flood and a high risk of damage from tropical cyclones on the more northerly coasts. In late 2010 and early 2011, unusually heavy rains caused several of the state’s major river systems to overrun their banks. The record flooding inundated cities including Rockhampton, Bundaberg, and Emerald, and crops across large areas of Queensland were destroyed.

Plant and animal life

Queensland has a highly varied flora and fauna. At one extreme are the tropical and subtropical rainforests, scattered in coastal and near-coastal valleys and ranges, with a remarkable diversity of plant and animal species; the northern rainforests collectively were designated a UNESCO World Heritage site in 1988. However, coastal areas are covered mainly by open eucalyptus forest and sparse woodland, with much land cleared for agriculture. Farther inland are the low woodlands of various acacia species (including brigalow, mulga, and gidgee or gidyea), with grasslands on heavier soils. Tough, spiky, tussocky spinifex grass dominates the arid, sparsely vegetated interior.

Because of its variety of habitats and its position in relation to migrations of species, Queensland has the greatest animal diversity of any state in the country. More than 70 species of marsupials—from the large red kangaroo to small marsupial mice, with a great variety of possums, including the cuscus—are found in Queensland. There are also dozens of species of bats and rodents, nearly 80 species of snakes, and more than 150 species of lizards, as well as saltwater and freshwater crocodiles. The hundreds of bird species include two large flightless birds, the emu of open country and the cassowary of the northern rainforests. Marine and freshwater fishes abound, including the colourful diversity of marine life on coral reefs and the unique freshwater lungfish. The Great Barrier Reef—the world’s largest structure created by living organisms—was Queensland’s first World Heritage site, designated in 1981; others named since then include Fraser Island (1992) off the southeastern coast and the fossil finds in Boodjamulla (Lawn Hill) National Park near the northern town of Riversleigh (1994). The latter site is paired with a similar fossil site near Naracoorte, S.Aus.

People

Population composition

Of the mainland Australian states, Queensland has one of the lowest proportions of persons born overseas, roughly one-sixth of the population in the early 21st century. Early post-World War II immigrants were more attracted to the larger southern cities, particularly where manufacturing employment was expanding rapidly. Especially since 1970, however, Queensland’s population grew quickly, mainly under the impetus of interstate migration but also with overseas contributions, notably from Vietnam and New Zealand.The Vietnamese community, concentrated in Brisbane, is prominent in retail, food, and professional industries. New Zealanders have congregated south of Brisbane in Logan and in the Gold Coast region, both of which have struggled with high rates of unemployment in some areas.

Some 3 percent of Queenslanders describe themselves as either Aborigines or Torres Strait Islanders. The majority of these people live in cities and towns, often as an underclass, struggling to maintain their cultural identity and economic well-being. Most of the remainder live in remote communities in the far north, where, locally, they are still in the majority.

Click anywhere inside the article to add text or insert superscripts, subscripts, and special characters.
You can also highlight a section and use the tools in this bar to modify existing content:

Add links to related Britannica articles!
You can double-click any word or highlight a word or phrase in the text below and then select an article from the search box.
Or, simply highlight a word or phrase in the article, then enter the article name or term you'd like to link to in the search box below, and select from the list of results.

Note: we do not allow links to external resources in editor.
Please click the Web sites link for this article to add citations for
external Web sites.